Identification of alteration zone and gold mineralization based on magnetic anomaly and 3D model of geomagnetic satellite data inversion of Mount Pongkor Area, West Java

N. R. Permana, B. Gunawan, A. A. Primastika, Dias Shafa, Dhika Faiz Fadrian, Fardhan Rafshan Zani
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Abstract

Mount Pongkor is one of the areas in Indonesia with the largest gold mineralization potential in Java. One of the geophysical methods to identify the distribution of gold mineralization zones is the geomagnetic method that utilizes magnetic properties in the subsurface due to the influence of rock magnetization. Geomagnetic research has been conducted at Mount Pongkor, Bogor Regency, West Java with an area of 22 x 17 km as much as 793 magnetic satellite data from the National Oceanic and Atmospheric Administration (NOAA) website that has been corrected daily. This study aims to determine the distribution of alteration zones and mineralization of the study area. The results showed that the RTP map shows the distribution of magnetic anomalies ranging from -4.786 – 4.663 nT, with high anomalies in the north-south direction associated with mineralization zones with anomaly values ranging from 1.881 – 4.663 nT and low anomalies in the north-south direction associated with rock alteration zones with anomaly values ranging from -4,786 - (-2.174) nT.  In the 3D inversion model, the alteration zone has an average depth of 350 - 2600 m from topography with susceptibility contrast values ranging from -0.35 - (- 0.25) SI and the mineralization zone has an average depth of 350 - 2800 m from topography with susceptibility contrast values of 0.25 - 0.35 SI.©2022 JNSMR UIN Walisongo. All rights reserved.
基于磁异常的西爪哇Pongkor山地区蚀变带与金矿化识别及地磁卫星数据反演三维模型
Pongkor山是印尼爪哇最具金矿化潜力的地区之一。地磁法是识别金矿化带分布的地球物理方法之一,它利用地下受岩石磁化影响而产生的磁性。在西爪哇茂物摄政的Pongkor山进行了地磁研究,面积为22 x 17公里,每天都有来自国家海洋和大气管理局(NOAA)网站的793个磁卫星数据被更正。本研究旨在确定研究区蚀变带的分布和成矿作用。结果表明:RTP图显示磁异常分布范围为-4.786 ~ 4.663 nT,南北方向与矿化带相关的高异常异常范围为1.881 ~ 4.663 nT,南北方向与岩石蚀变带相关的低异常异常范围为- 4786 ~ (-2.174)nT。蚀变带距离地形的平均深度为350 ~ 2600 m,磁化率对比值为-0.35 ~ (- 0.25)SI;矿化带距离地形的平均深度为350 ~ 2800 m,磁化率对比值为0.25 ~ 0.35 SI。©2022 JNSMR UIN Walisongo。版权所有。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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